Combined planktic foraminifera assemblage records and organic carbon content in sediment core SSD-044/GC-01

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Hauptverfasser: Yadav, Ramanand, Naik, Sushant S, Narvekar, Jayu
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2022
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author Yadav, Ramanand
Naik, Sushant S
Narvekar, Jayu
author_facet Yadav, Ramanand
Naik, Sushant S
Narvekar, Jayu
collection Datos científicos de ciencias marinas y ambientales
contents We have utilized the ratio of mixed layer eutrophic to mixed layer oligotrophic foraminifer species, thermocline foraminifera species, and sedimentary organic carbon (C-org) content from the core SSD-044/GC01 to infer the Mixed layer and Thermocline variability during late glacial to Holocene. The mixed layer increases, and the thermocline deepens during Last Glacial Maximum (LGM) and vice versa during the last deglacial and Holocene which is influenced by the coupling of northeast (NE)/southwest (SW) Monsoon.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_946305
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Combined planktic foraminifera assemblage records and organic carbon content in sediment core SSD-044/GC-01
Yadav, Ramanand
Naik, Sushant S
Narvekar, Jayu
AGE; Carbon, organic; Central equatorial Indian Ocean; Counting, stereo microscope; DEPTH, sediment/rock; Element analyser CHNS; Equatorial Indian Ocean; Eutrophic species; GC; Gravity corer; Last Glacial Maximum; Oligotrophic species; Planktic foraminifera assemblage; productivity; Sindhu Sadhana; SSD-044; SSD044_GC-01; Winter monsoon
We have utilized the ratio of mixed layer eutrophic to mixed layer oligotrophic foraminifer species, thermocline foraminifera species, and sedimentary organic carbon (C-org) content from the core SSD-044/GC01 to infer the Mixed layer and Thermocline variability during late glacial to Holocene. The mixed layer increases, and the thermocline deepens during Last Glacial Maximum (LGM) and vice versa during the last deglacial and Holocene which is influenced by the coupling of northeast (NE)/southwest (SW) Monsoon.
title Combined planktic foraminifera assemblage records and organic carbon content in sediment core SSD-044/GC-01
topic AGE; Carbon, organic; Central equatorial Indian Ocean; Counting, stereo microscope; DEPTH, sediment/rock; Element analyser CHNS; Equatorial Indian Ocean; Eutrophic species; GC; Gravity corer; Last Glacial Maximum; Oligotrophic species; Planktic foraminifera assemblage; productivity; Sindhu Sadhana; SSD-044; SSD044_GC-01; Winter monsoon
url https://doi.org/10.1594/PANGAEA.946305